Determining NMR flow propagator moments in porous rocks without the influence of relaxation

Flow propagators, used for the study of advective motion of brine solution in porous carbonate and sandstone rocks, have been obtained without the influence of Nuclear Magnetic Resonance (NMR) relaxation times, T 1 and T 2. These spin relaxation mechanisms normally result in a loss of signal that va...

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Veröffentlicht in:	Journal of magnetic resonance (1997) 2008-08, Vol.193 (2), p.218-225
Hauptverfasser:	Mitchell, J., Graf von der Schulenburg, D.A., Holland, D.J., Fordham, E.J., Johns, M.L., Gladden, L.F.
Format:	Artikel
Sprache:	eng
Schlagworte:	Algorithms Diffusion Displacement-T2 correlation Flow Geologic Sediments - analysis Geologic Sediments - chemistry Laplace–Fourier transform Magnetic Resonance Spectroscopy - methods Permeable rocks Propagators Relaxation Rheology - methods Salts - analysis Salts - chemistry T1-displacement correlation
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